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2.5 Geochemistry  101
                         almost impossible to find a solution to corrosion and scaling problems except on a
                         specific basis for particular sites.
                           The chemistry from different fields can vary substantially. Higher temperature
                         resources with the higher water ratios have increased levels of silica that cause
                         tremendous scaling and deposit problems. By contrast, dry steam fields do not
                         experience the silica problems, but instead have aggressive corrosion problems as-
                         sociated with hydrogen chloride and hydrogen sulfide attack. Still other geothermal
                         fields are hit with a double misfortune and encounter both scaling and corrosion
                         problems at thesametime(Figure2.20).
                           Corrosion attacks occur in many geothermal operations and these result in severe
                         equipment damage (Lichti and Wilson, 1999). Corrosion may be general, a sort
                         of ‘‘rusting’’ that affects all metal surfaces in geothermal equipment, or localized.
                         There are multiple mechanisms, for example, stress corrosion and sulfide stress
                         cracking, of corrosion attack contributing to the failure of pipe and equipment in
                         these systems (Corsi, 1986). The first is due to stress coupled with the existence
                         of chloride ions in the environment and the second is caused by the presence
                         of hydrogen sulfide in an aqueous phase. The thermal and hydraulic machines
                         require materials that can withstand stress as well as corrosion erosion resulting






































                         Figure 2.20  Wellheadsubmittedtocorrosion andscaling. (PhotoF.-D. Vuataz).
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